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BRITISH GEOLOGICAL SURVEY TECHNICAL REPORT WA/95/13 Onshore Geology Series TECHNICAL REPORT WA/95/13 Geology of the Brixton Deverill-East Knoyle district (Wiltshire) 1:lO 000 sheets ST 83 NE (Brixton Deverill) and ST 83 SE (East Knoyle) Part of l:5O 000 Sheet 297 (Wincanton) C R Bristow Contributors B M Cox (Jurassic biostratigraphy) and M A Woods (Cretaceous biostratigraphy) Geographical index UK, SW England, Wiltshire Subject index Geology, Jurassic, Kimmeridge Clay Cretaceous, Upper Greensand, Chalk Bibliographical reference Bristow, C R. 1995. Geology of the Brixton Deverill-East Knoyle district (Wiltshire). 1:lO 000 sheets ST 83 NE and ST 83 SE. British Geological Survey Technical Report WA/95/13 @ NERC Copyright 1995. Exeter, British Geological Survey 1995 PREFACE This account describes the geology depicted on 1:lO 000 sheets ST83NE (Brixton Deverill and ST83SE (East Knoyle), which form part of the l:5O 000 Wincanton (297) Sheet. The district was first geologically survyed on the one-inch scale by H W Bristow in 1852 as part of Old Series Sheet 15, published in 1856, and W T Aveline (date unknown) as part of Old Series Sheet 14, published in 1857. A revised edition of Sheet 14 was issued in 1859. Revision of the Cretaceous strata at the 1:lO 560 scale was carried out by A J Jukes-Browne in 1889 and 1890, and by F J Bennett in 1894-1896. Mr B H Mottram surveyed the area of the Mere Fault and associated disturbance at the 1:lO 560 scale in 1950 and 1951 and published the results in the Proceedings of the Geologists' Association in 1961; he later donated his maps to the BGS. A Provisional edition, at the 1:63 360 scale, of the Wincanton Sheet, based on Old Series sheets 14 and 15 and Mottram's mapping, was published in 1969. The sheet was reprinted at the l:5O 000 scale without geological revision in 1972. The 1:lO 000-scale revision survey of the district was carried out by C R Bristow in 1994 under the direction of R W Gallois and I R Basham, Regional Geologists. Cretaceous macrofossils have been identified by M A Woods. Dyeline black and white copies of the geological maps can be ordered from the British Geological Survey, Keyworth. CONTENTS Page 1. INTRODUCTION 1 2. JURASSIC Kimmeridge Clay Portland Group Wardour Formation Portland Stone Formation Tisbury Member 3. CRETACEOUS 9 Gault 9 Upper Greensand 10 Cann Sand 10 Shaftesbury Sandstone 10 Boyne Hollow Chert 11 Melbury Sandstone 11 Details 11 Chalk Group 14 Lower Chalk 14 West Melbury Marly Chalk 15 Zig Zag Chalk 15 Middle Chalk 15 Holywell Nodular Chalk 15 New Pit Chalk 16 Upper Chalk 16 Lewes Nodular Chalk 16 Seaford Chalk 17 Details 1.7 4. STRUCTURE 27 5. DRIFT Clay-with-flints Older Head Head Undifferentiated River Terrace Deposits First River Terrace Deposits Alluvium Lands lips Swallowholes 6. ECONOMIC DEPOSITS Building Stone Roads tone 31 Lime and Mar1 31 Brick Clay 31 7. REFERENCES 32 Appendix 1. Palaeontological reports relevant to the district 33 Figures 1. Geological sketch-map of the Brixton Devrill-East Knoyle 3 2. Sketch-map of the landslips and Kimmeridge Clay in the West Knoyle area 5 3. Sketch of hardgrounds in the Chalk Rock 22 4. Section in the Lewes Chalk at the East Knoyle Chalk pit [8875 31101 (based on Jukes-Browne and Hill (1904) and Woods (1994~)) 25 5. Sketch-map of the Mere Fault and associated monoclinal structure 28 Tables 1. Geological succession in the Brixton Deverill-East Knoyle area 2 1.INTRODUCTION The Brixton Deverill-East Knoyle district lies at the western endof Salisbury Plain and encompasses the north-western part of the Vale of Wardour. The central part of the district forms part of a dissected plateau developed on Upper Chalk (Figure 1); this reaches a maximum height of 238 m south-east of Brixton Deverill. In the north-west, there are prominent escarpments capped by the Lewes Chalk on either side of the Wylye valley. In the south, the Mere Fault and associated monoclinal structure play an important part in shaping the landscape. In the west, the chalk rises steeply on the north side of the fault from the clay vale to the south. Between West Knoyle and East Knoyle, the steeply dipping Upper Greensand and Chalk strata give rise to strongly featured ground. The principal drainage in the northern part of the district is northwards by the River Wylye, the only permanent river on the chalk outcrop and its tributaries. In the south-central area, drainage is eastwards by a series of valleys that coalesce just west of Hindon and ultimately join the River Nadder at Tisbury. In the south, on the clay vale, drainage is south- westwards by tributaries of the River Lodden, and south-eastwards by tributaries of the River Nadder. The lowest point in the district, c.96 m OD, lies in the southern tract. Soils developed on the Upper Greensand and most of the Chalk are light and well drained. However, soils on the West Melbury Chalk, together with some on the clay-with-flint deposits and Kimmeridge Clay are much heavier and poorly drained. Agriculture is a mixture of arable and pasture, with the latter dominant on the Kimmeridge Clay Vale. There are few woods, with deciduous woods confined mostly to the clay vale and the relatively newly planted coniferous plantations on the Chalk and Upper Greensand. Agriculture is the only industry in the area. The soild formations and drift deposits on the 1:lO 000 geological sheets ST83NE and SE are shown in Table 1. 1 Table 1. Geological succession in the Brixton Deverill-East Knoyle district Drift deposits Landslip Alluvium River Terrace Deposits Undifferentiated River Terrace Deposits Head Older Head Clay-with-flints So 1 id Deposits Thickness (m) Chalk Seaford Chalk 45 Lewes Nodular Chalk 25-33 New Pit Chalk 12-15 Holywell Nodular Chalk 12-15 Zig Zag Chalk 10-25 West Melbury Chalk 15-40 Upper Greensand Melbury Sandstone 1-5 Boyne Hollow Chert 9-12 Shaftesbury Sandstone 1-5 Cann Sand 12 Gault 18 Portland Group Tisbury Member 10 Wardour Formation 15 Kimmeridge Clay 185 2 e I I. I I I Seaford Chalk LeCk Lewes Nodular Chalk Middle Chalk Zig Zag Chalk West Melbury Marly Chalk Upper Greensand Gault Kimmeridge Clay /-Fault, crossmark on downthrow side Figure 1, Sketch-map of the solid geology of the Brixton D everill - East Knoyle district 2. JURASSIC Kimmeridge Clay About 185 m of Kimmeridge Clay crop out in the southern part of the district, of which about 30 m belong to the upper part of the Lower Kimmeridge Clay and the rest to the Upper Kimmeridge Clay. The formation consists dominantly of medium grey, fissile, shelly mudstones, and medium and brownish grey, bituminous shelly mudstones ('oil- shale'). Cementstone beds occur at intervals and appear to form mappable features at three principal levels (Figure 2). The lowest, which is exposed in the stream bed [8653 30761 north-east of Lugmarsh Farm, is a lobate, dense, ?ferroan, highly septarian cementstone which appears to fall in the basal part of KC35 or in the top part of KC34 (at about the level of the Maple Ledge Stone Band of the Dorset coast). The second cementstone, which occurs about 5 m higher, is exposed in the stream bed [8608 31221 north of Lugmarsh Farm, It is a 15 cm thick, brownish grey, densely cemented, septarian cementstone with a fluted top. It is overlain by a fissile, shelly, oil shale. The exact position of this cementstone (Figure 2, locality 8) within the Kimmeridge Clay is problematical as the associated fauna (see details) indicates KC37 near the base of the Upper Kimmeridge Clay (and therefore Yellow Ledge Stone Band), which conflicts with the evidence of nearby faunas downstream [8599 31151 (Figure 2, locality 7) and upstream [8610 3131 and 8613 31371 (Figure 2, localities 9 and 10). Locality 10 yielded the ammonite AuZacostephanUs, and is therefore firmly fixed in the Lower Kimmeridge Clay (KC35 or below). A presumed cementstone, some 13 m higher than the second, forms an excelIent feature across the present area and on to the adjacent district to the south where it was thought to represent the Yellow Ledge Stone Band at the base of KC37 (Bristow, 1993). However, in the present area, fauna1 evidence suggests that feature represents a stratigraphically lower level than the Yellow Ledge Stone Band, and possibly lies at the Lower/Upper Kimmeridge Clay boundary (i.e. Blake's Bed 42 of the Dorset coast). The oldest strata, belonging to the Eudoxus Zone (KC3O), crop out in the unnamed stream on the extreme west of the district, south-west of West Knoyle [8504 31821 (Figure 2, localities 1-2). Younger strata, belonging to the Autissiodorensis Zone, have been recognised in streams south-west, south, and south-east of West Knoyle. 4 -31 West Knoyle area Although some 155 m of Upper Kimmeridge Clay crop out in the district, there is no undoubted exposure in this unit. There are possible occurrences of the basal bed (KC36) of the Upper Kimmeridge Clay in two streams [8610 3131 and 8657 30851, but the fauna1 evidence is equivocal (see Details) and it is thought more likely that these two localities fall in the top part of KC35. One possible occurrence of KC37 [8608 31221 has been mentioned above. Details In the stream west of Broadmead Farm, West Knoyle, moderately fissile, medium to pale grey, moderately shelly and shelly mudstones with Nanogyra virguta, Protocardia and rare Amoeboceras (Nannocardioceras) krausei crop out [8504 3182](Figure 2, locality 1).